ClimateSearch

Kakogawachō-honmachi, Hyōgo

Japan · 272k people · 7 m elevation · Northern Hemisphere

Every month in detail

Thirty-year averages for each calendar month.

Monthly climate normals. Values shown as an em dash are missing from the source data.
MonthJanFebMarAprMayJunJulAugSepOctNovDec
Average high48°F (9°C)50°F (10°C)56°F (14°C)67°F (19°C)75°F (24°C)81°F (27°C)88°F (31°C)91°F (33°C)83°F (29°C)73°F (23°C)63°F (17°C)53°F (12°C)
Average low33°F (0°C)33°F (1°C)38°F (4°C)47°F (9°C)57°F (14°C)66°F (19°C)74°F (23°C)75°F (24°C)68°F (20°C)57°F (14°C)46°F (8°C)36°F (2°C)
Dew point31°F (0°C)32°F (0°C)37°F (3°C)47°F (8°C)56°F (14°C)65°F (18°C)73°F (23°C)74°F (23°C)66°F (19°C)56°F (13°C)46°F (8°C)36°F (2°C)
Rainfall1.8 in (45 mm)2.2 in (55 mm)3.7 in (94 mm)4.6 in (116 mm)5 in (127 mm)6.7 in (170 mm)6.4 in (162 mm)3.6 in (92 mm)7.3 in (186 mm)5.2 in (131 mm)2.5 in (65 mm)2 in (52 mm)
Rainy days569999859866
Snowfall0.3 in (0.7 cm)1 in (2.6 cm)0.1 in (0.2 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0 in (0 cm)0.1 in (0.3 cm)
Sunshine171 h159 h179 h176 h183 h132 h170 h219 h172 h177 h166 h171 h

Scroll the table sideways for all twelve months.

Projected change, 2031–2050

Model projection, not an observation

How this city’s climate may change, measured against the same models’ own 1995–2014 output. Nothing here affects the match score above.

Change in summer afternoon highs

+2.3°F (+1.3°C)

Models range from +1.7°F (+1.0°C) to +2.7°F (+1.5°C)

Days above 90°F (32°C) a year

—

Too few hot days today to project a reliable change

Warming by month
  • January: +2.1°F (+1.1°C)
  • February: +1.8°F (+1.0°C)
  • March: +1.7°F (+1.0°C)
  • April: +2.3°F (+1.3°C)
  • May: +1.9°F (+1.1°C)
  • June: +2.2°F (+1.2°C)
  • July: +2.4°F (+1.3°C)
  • August: +2.2°F (+1.2°C)
  • September: +2.8°F (+1.5°C)
  • October: +2.8°F (+1.5°C)
  • November: +2.6°F (+1.5°C)
  • December: +2.3°F (+1.3°C)
Scenario
SSP5-8.5 (high emissions)
Models
4 · CMIP6 HighResMIP, downscaled

This is a high-emissions pathway — the upper end of plausible futures, not a central estimate. Changes are measured by each model against its own past output and then applied to the observed record, which cancels each model’s bias but not the genuine uncertainty about how much warming occurs. Where the models disagree widely, the range above is the honest answer.